Preface

It is suggested to introduce new standard names for several tidal
quantities like (tidal) high_water, low_water etc. These are geophysical
concepts and it would be not adequate to describe them with cell_methods
and/or time bounds.

---
1.) tidal_high_water_level_above_sea_level [ m ]

    The maximum height reached by a rising tide. The high water is due
    to the periodic tidal forces and the effects of meteorological,
    hydrologic, and/or oceanographic conditions. Sea_level means mean
    sea level, which is close to the geoid in sea areas.


---
2.) tidal_low_water_level_above_sea_level [ m ]

    The minimum height reached by a falling tide. The low water is due
    to the periodic tidal forces and the effects of meteorological,
    hydrologic, and/or oceanographic conditions. Sea_level means mean
    sea level, which is close to the geoid in sea areas.


---
3.) tidal_range [ m ]

    Arithmetic mean between tidal rise and tidal fall. Due to the periodic
    tidal forces and the effects of meteorological, hydrologic, and/or
    oceanographic conditions.


---
4.) half_tide_level_above_sea_level [ m ]

    Water level at half tidal range. The level midway between high
    water and mean low water for a tide. Due to the periodic tidal
    forces and the effects of meteorological, hydrologic, and/or
    oceanographic conditions. Sea_level means mean sea level, which is
    close to the geoid in sea areas.


---
5.) mean_tide_water_level_above_sea_level [ m ]

    The mean surface elevation as determined by averaging the heights
    of the water at equal intervals of time for a tidal period, which is
    the interval between two successive low waters. Differs
    from half tide level due to tidal asymmetry. Due to the periodic tidal
    forces and the effects of meteorological, hydrologic, and/or
    oceanographic conditions. Sea_level means mean sea level, which is
    close to the geoid in sea areas.


---
6.) mean_tidal_rise_water_level_above_sea_level [ m ]
    (opt) mean_flood_water_level_above_sea_level [ m]

    The mean surface elevation as determined by averaging the heights
    of the water at equal intervals of time for the period of tidal rise,
    which is the interval from low water to high water.
    Differs from mean water level during tidal fall due to tidal
    asymmetry. Due to the periodic tidal forces and the effects of
    meteorological, hydrologic, and/or oceanographic conditions.
    Sea_level means mean sea level, which is close to the geoid in
    sea areas.


---
7.) mean_tidal_fall_water_level_above_sea_level [ m ]
    (opt) mean_ebb_water_level_above_sea_level [ m]

    The mean surface elevation as determined by averaging the heights
    of the water at equal intervals of time for the period of tidal fall,
    which is the interval from high water to low water.
    Differs from mean water level during tidal rise due to tidal
    asymmetry. Due to the periodic tidal forces and the effects of
    meteorological, hydrologic, and/or oceanographic conditions.
    Sea_level means mean sea level, which is close to the geoid in
    sea areas.


---
8.) duration_of_tidal_rise [ s ]

   Duration of rise is the interval from low water to high water. In
   combination with duration_of_tidal_fall they cover, on an average,
   a period of 12.42 hours for a semidiurnal tide or a period of 24.84
   hours for a diurnal tide. In a normal semidiurnal tide, duration of
   rise and duration of fall each will be approximately equal to 6.21
   hours, but in shallow waters and in rivers there is a tendency for
   a decrease in duration of rise and a corresponding increase in
   duration of fall. Due to the periodic tidal forces and the effects
   of meteorological, hydrologic, and/or oceanographic conditions.


---
9.) duration_of_tidal_fall [ s ]

  Duration of fall is the interval from high water to low water. In
  combination with duration_of_tidal_rise they cover, on an average,
  a period of 12.42 hours for a semidiurnal tide or a period of 24.84
  hours for a diurnal tide. In a normal semidiurnal tide, duration of
  rise and duration of fall each will be approximately equal to 6.21
  hours, but in shallow waters and in rivers there is a tendency for
  a decrease in duration of rise and a corresponding increase in
  duration of fall. Due to the periodic tidal forces and the effects
  of meteorological, hydrologic, and/or oceanographic conditions.


---
10.) duration_of_tide [ s ]
     (opt) tidal_period [ s ]

  Interval between two successive low waters. Sum of duration_of_tidal_rise
  and duration_of_tidal_fall. On an average, a period of 12.42 hours for
  a semidiurnal tide or a period of 24.84 hours for a diurnal tide. Due
  to the periodic tidal forces and the effects of meteorological,
  hydrologic, and/or oceanographic conditions.


---
11.) time_of_occurrence_of_tidal_high_water [ s ]

  Time when high water occurs. Due to the periodic tidal forces and
  the effects of meteorological, hydrologic, and/or oceanographic
  conditions.


---
12.) time_of_occurrence_of_tidal_low_water [ s ]

  Time when low water occurs. Due to the periodic tidal forces and
  the effects of meteorological, hydrologic, and/or oceanographic
  conditions.


---
13.) tidal_difference_for_time_of_occurrence_of_tidal_high_water [ s ]

  Difference in time of a high water at a subordinate station and at
  a reference station. The difference, when applied according to sign
  to the time at the reference station, gives the corresponding time
  for the subordinate station. Due to the periodic tidal forces and
  the effects of meteorological, hydrologic, and/or oceanographic
  conditions.


---
14.) tidal_difference_for_time_of_occurrence_of_tidal_low_water [ s ]

  Difference in time of a low water at a subordinate station and at
  a reference station. The difference, when applied according to sign
  to the time at the reference station, gives the corresponding time
  for the subordinate station. Due to the periodic tidal forces and
  the effects of meteorological, hydrologic, and/or oceanographic
  conditions.


---
15.) tidal_rise [ m ]

  Vertical difference between the water level at low water and the
  water level at the subsequent high water. Due to the periodic tidal
  forces and the effects of meteorological, hydrologic, and/or
  oceanographic conditions.


---
16.) tidal_fall [ m ]

  Vertical difference between the water level at high water and the
  water level at the subsequent low water. Due to the periodic tidal
  forces and the effects of meteorological, hydrologic, and/or
  oceanographic conditions.


---
17.) duration_of_wetting_due_to_tidal_flooding [ s ]

  Duration for which a location is covered with water due to tidal
  flooding. Within the intertidal zone, flooding may last from 0.00
  (always dry) up to, on an average, 12.42 hours (always wet) for a
  semidiurnal tide. Or up to, on an average, 24.84 hours for a diurnal
  tide. Due to the periodic tidal forces and the effects of
  meteorological, hydrologic, and/or oceanographic conditions.


---
18.) duration_of_drying_due_to_tidal_ebbing [ s ]

  Duration for which a location is not covered with water due to tidal
  ebbing. Within the intertidal zone, ebbing may last from 0.00
  (always wet) up to, on an average, 12.42 hours (always dry) for a
  semidiurnal tide. Or up to, on an average, 24.84 hours for a diurnal
  tide. Due to the periodic tidal forces and the effects of
  meteorological, hydrologic, and/or oceanographic conditions.


Günther Lang

Bundesanstalt für Wasserbau - Dienststelle Hamburg
Referat Ästuarsysteme II
Wedeler Landstraße 157
22559 Hamburg
Telefon +49 (0) 40 81908 360
E-Mail guenther.l...@baw.de
BEGIN:VCARD
VERSION:3.0
PRODID:OPEN-XCHANGE
FN:Lang\, Günther
N:Lang;Günther;;Dr.-Ing.;
X-OPEN-XCHANGE-CTYPE:contact
ADR;TYPE=work:;;Wedeler Landstraße 157;Hamburg;;22559;
TEL;TYPE=work,voice:+49 (40) 81908-360
TEL;TYPE=work,fax:+49 (40) 81908-373
EMAIL;TYPE=INTERNET,work:guenther.l...@baw.de
ORG:BAW;K3
REV:20131126T120035.482Z
UID:0300a0fa-664e-4c72-8b07-eb6f297f244c
END:VCARD
_______________________________________________
CF-metadata mailing list
CF-metadata@cgd.ucar.edu
http://mailman.cgd.ucar.edu/mailman/listinfo/cf-metadata

Reply via email to